Shaw Jeremy A, Macey David J, Brooker Lesley R, Stockdale Edward J, Saunders Martin, Clode Peta L
Centre for Microscopy, Characterisation and Analysis, The University of Western Australia, Crawley, WA 6009, Australia.
Microsc Microanal. 2009 Apr;15(2):154-65. doi: 10.1017/S1431927609090230.
The cusp epithelium is a specialized branch of the superior epithelium that surrounds the developing teeth of chitons and is responsible for delivering the elements required for the formation of biominerals within the major lateral teeth. These biominerals are deposited within specific regions of the tooth in sequence, making it possible to conduct a row by row examination of cell development in the cusp epithelium as the teeth progress from the unmineralized to the mineralized state. Cusp epithelium from the chiton Acanthopleura hirtosa was prepared using conventional chemical and microwave assisted tissue processing, for observation by light microscopy, conventional transmission electron microscopy (TEM) and energy filtered TEM. The onset of iron mineralization within the teeth, initiated at row 13, is associated with a number of dramatic changes in the ultrastructure of the apical cusp cell epithelium. Specifically, the presence of ferritin containing siderosomes, the position and number of mitochondria, and the structure of the cell microvilli are each linked to aspects of the mineralization process. These changes in tissue development are discussed in context with their influence over the physiological conditions within both the cells and extracellular compartment of the tooth at the onset of iron mineralization.
齿尖上皮是上皮组织的一个特殊分支,围绕石鳖发育中的牙齿,负责为主要侧齿内生物矿物质的形成提供所需成分。这些生物矿物质按顺序沉积在牙齿的特定区域,随着牙齿从未矿化状态发展到矿化状态,使得对齿尖上皮中细胞发育进行逐行检查成为可能。使用传统化学和微波辅助组织处理方法制备了石鳖多棘艾氏石鳖的齿尖上皮,用于光学显微镜、传统透射电子显微镜(TEM)和能量过滤TEM观察。牙齿中铁矿化从第13排开始,与顶端齿尖细胞上皮超微结构的一些显著变化相关。具体而言,含铁小体的铁蛋白的存在、线粒体的位置和数量以及细胞微绒毛的结构都与矿化过程的各个方面相关。结合这些变化对铁矿化开始时牙齿细胞内和细胞外区室生理条件的影响,讨论了组织发育中的这些变化。